[1]Schulz H. Short history and present trends of Fischer-Tropsch synthesis[J].Applied Catalysis A: General,1999, 186: 3-12.
[2]Davis B H. Overview of reactors for liquid phase Fischer-Tropsch synthesis[J]. Catalysis Today,2002, 71: 249-300.
[3]Suo Zhanghuai, Kou Yuan, Wang Hongli. Recent progress in catalytic synthesis of C⁺₂ hydrocarbons from CO₂ [J]. Natural Gas Chemical Industry,1998, 23(1): 51-56. [索掌怀, 寇元,王弘立. CO₂催化合成C⁺₂烃新进展[J].天然气化工,1998,23（1）：51-56.]
[4]Riedel T, Claeys M, Schulz H, et al. Comparative study of Fischer-Tropsch synthesis with H₂/CO and H₂/CO₂ syngas using Fe- and Co-based catalysts [J]. Applied Catalysis A: General,1999, 186: 201-213.
[5]Trovarelli A, Mustazza C, DolcettiJan G, et al. Carbon dioxide hydrogenation on rhodium supported on transition metal oxides : Effect of reduction temperature on product distribution [J]. Applied Catalysis,1990, 65(1): 129-142.
[6]Chang F W, Kuo M S, Tsay M T, et al. Hydrogenation of CO₂ over nickel catalysts on rice huskash-alumina prepared by incipient wetness impregnation [J]. Applied Catalysis A: General,2003,247: 309-320.
[7]Lee S C, Jang J H, Lee B Y, et al. Promotion of hydrocarbon selectivity in CO₂ hydrogenation by Ru component [J]. Journal of Molecular Catalysis A: Chemical,2004, 210: 131-141.
[8]Moody J B. Serpentinization: A review [J]. Lithos,1976, 9: 125-138.
[9]Neal C, Stanger G. Hydrogen generation from mantle source rocks in Omen [J]. Earth and Planetary Science Letters,1983, 66: 315-320.
[10]Janecky D R, Seyfried Jr W E. Hydrothermal serpentinization of peridotite within the oceanic crust: Experimental investigations of mineralogy and major element chemistry [J]. Geochimica et Cosmochimica Acta,1986, 50: 1 357-1 378.
[11]Chen Youyi. Origins of carbon dioxide in petroliferous basins[J]. Advances in Earth Science,2000, 15(6): 684-687. [程有义.含油气盆地二氧化碳成因研究[J].地球科学进展,2000,15(6):684-687.]
[12]Holloway J R, O’Day P A. Production of CO₂ and H₂ by diking-eruptive events at mid-ocean ridges: Implications for abiotic organic synthesis and global geochemical cycling[J].International Geology Review,2000, 42: 673-683.
[13]Resing J A, Lupton J E, Feely R A, et al. CO₂ and ³He in hydrothermal plumes: Implications for mid-ocean ridge CO₂ flux[J]. Earth and Planetary Science Letters,2004, 226: 449-464.
[14]Welhan J A. Origin of methane in hydrothermal systems [J]. Chemical Geology,1988, 71: 183-198.
[15]Botz R, Stuben D, Winckler G, et al. Hydrothermal gases offshore Milos Island, Greece [J]. Chemical Geology,1996, 130: 161-173.
[16]Charlou J L, Bougault H, Appriou P, et al. Different TDM/CH₄ hydrothermal plume signatures: TAG site at 26°N and serpentinized ultrabasic diapir at 15°05′N on the Mid-Atlantic ridge[J]. Geochimica et Cosmochimica Acta,1991, 55: 3 209-3 223.
[17]Rona P A, Bougault H, Charlou J L, et al. Hydrothermal circulation, serpentinization, and degassing at a rift valley-fracture zone intersection: Mid-Atlantic ridge near 15°N, 45°W[J]. Geology,1992, 20: 783-786.
[18]Charlou J L, Fouquet Y A, Bougault H, et al. Intense CH₄ degassing generated by serpentization of ultramafic rocks at the intersection of the 15°20′N fracture zone and the Mid-Atlantic Ridge [J]. Geochimica et Cosmochimica Acta, 1998, 62:2 323-2 333.
[19]Charlou J L, Donval J P, Fouquet Y, et al. Geochemistry of high H₂ and CH₄ vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal field (36°14′N, MAR) [J]. Chemical Geology,2002, 191:345-359.
[20]Holm N G, Charlou J L. Initial indications of abiotic formation of hydrocarbons in the Rainbow ultramafic hydrothermal system, Mid-Atlantic Ridge [J]. Earth and Planetary Science Letters, 2001, 191:1-8.
[21]Szatmari P. Petroleum formation by Fischer-Tropsch synthesis in plate tectonics [J]. The American Association of Petroleum Geologists Bulletin,1989, 73(8): 989-998.
[22]Zhang Jinglian, Zhang Pingzhong, Lü Ximin, et al. New advance of inorganic origin on petroleum[J]. Advances in Earth Science,1998, 13(1): 44-50. [张景廉, 张平中, 吕锡敏, 等. 油气无机成因学说的新进展[J]. 地球科学进展, 1998, 13（1）：44-50.]
[23]Lü Gongxuan, Chou Linjun, Zhang Bing, et al. Formation on mechanism of abiogenic of hydrocarbons and organics generation in deep strata [J]. Natural Gas Geoscience,2006, 17(1): 14-18. [吕功煊, 丑凌军, 张兵, 等. 深层及非生物成烃的催化机制[J]. 天然气地球科学, 2006, 17（1）：14-18.]
[24]Corliss J B, Baross J A, Hoffman S E. An hypothesis concerning the relationship between submarine hot springs and the origin of life on Earth [J]. Oceanologica Acta,1981, 4(SP): 59-69.
[25]Joyce G. Hydrothermal vents too hot? [J]. Nature,1988, 334: 564.
[26]Miller S L, Bada J S. Submarine hot spring and the origin of life [J].Nature,1988, 334: 609-611.
[27]Corliss J B. The flow of energy, natural learning system and the creation of life on earth [J]. Acta Astronautica,1989, 19(11): 869-873.
[28]Corliss J B. Hot spring and the origin of life [J]. Nature,1990, 347: 624.
[29]McCollom T M, Ritter G, Simoneit B R T. Lipid synthesis under hydrothermal conditions by Fischer-Tropsch-Type reactions [J]. Origins of Life and Evolution of the Biosphere,1999, 29: 153-166.
[30]Shock E L, Schulte M D. Organic synthesis during fluid mixing in hydrothermal systems [J]. Journal of Geophysical Research,1998, 103(E12): 28 513-28 537.
[31]Simoneit B R T. Prebiotic organic synthesis under hydrothermal conditions: An overview [J]. Advances in Space Research,2004, 33: 88-94.
[32]Helgeson H C, kirkham D H. Theoretical prediction of the thermodynamic behavior of aqueous electrolytes at high pressures and temperatures: Ⅰ  Summary of the thermodynamic/electrostatic properties of the solvent [J]. American Journal of Science,1974, 274: 1 089-1 198.
[33]Helgeson H C, Kirkham D H, Flowers G C. Theoretical prediction of the thermodynamic behavior of aqueous electrolytes at high pressures and temperatures: Ⅳ Calculation of activity coefficients, osmotic coefficients, and apparent molal and standard and relative partial molal properties to 600℃ and 5kb [J]. American Journal of Science,1981, 281: 1 249-1 516.
[34]Shock E L, Helgeson H C, Sverjensky D A. Calculation of the thermodynamic and transport properties of aqueous species at high pressures and temperatures: Standard partial molal properties of inorganic neutral species [J]. Geochimica et Cosmochimica Acta,1989, 53: 2 157-2 183.
[35]Johnson J W, Norton D. Critical phenomena in hydrothermal systems: state, thermodynamic, and transport properties of H₂O in the critical region [J]. American Journal of Science, 1991, 291: 541-648.
[36]Shock E L, Helgeson H C. Calculation of the thermodynamic and transport properties of aqueous species at high pressures and temperatures: Standard partial molal properties of organic species [J]. Geochimica et Cosmochimica Acta, 1990, 54: 915-945.
[37]Johnson J M, Oelkers E H, Helgeson H C. SUPCRT 92: A software package for calculating the standard molal thermodynamic properties of minerals, gases, aqueous species, and reactions from 1 to 5 000 bar and 0 to 1 000℃ [J]. Computers & Geosciences, 1992, 18(7): 899-947.
[38]McCollom T M, Seewald J S. A reassessment of the potential for reduction of dissolved CO₂ to hydrocarbons during serpentinization of olive [J]. Geochimica et Cosmochimica Acta,2001, 65(21): 3 769-3 778.
[39]Berndt M E, Allen D E, Seyfried Jr W E. Reduction of CO₂ during serpentinization of olive at 300℃ and 500 bar [J]. Geology,1996, 24(4):351-354.
[40]Horita J, Berndt M E. Abiogenic methane formation and isotopic fractionation under hydrothermal conditions [J]. Science,1999, 285:1 055-1 057.
[41]Foustoukos D I, Seyfried Jr W E. Hydrocarbons in hydrothermal vent fluids: The role of chromium-bearing catalysts [J]. Science,2004, 304:1 002-1 005.
[42]McCollom T M, Seewald J S. Experimental constraints on the hydrothermal reactivity of organic acids and anions: Ⅰ. Formic acid and formate [J]. Geochimica et Cosmochimica Acta,2003, 67(19):3 625-3 644.
[43]Seewald J S, Zolotov M Y, McCollom T M. Experimental investigation of single carbon compounds under hydrothermal conditions [J]. Geochimica et Cosmochimica Acta,2006, 70: 446-460.
[44]Dai Jinxing. Identification and distinction of various alkane gases[J].Science in China(Series B),1992,（2）：185-193.[戴金星. 各类烷烃气的鉴别[J]. 中国科学:B辑, 1992,（2）：185-193.]
[45]Wang Xianbin, Li Chunyuan, Chen Jianfa, et al. On abiogenic natural gas[J].Chinese Science Bulletin,1997, 42(12): 1 233-1 241.[王先彬, 李春园, 陈践发, 等. 论非生物成因天然气[J].科学通报, 1997, 42（12）：1 233-1 241.]
[46]Hu Guixing, Ou Yang Ziyuan, Wang Xianbin, et al. Carbon isotope fractionation in the process of Fischer-Tropsch reaction in primitive solar nebula [J]. Science in China (Series D),1998, 41(2): 202-207. [胡桂兴, 欧阳自远, 王先彬, 等. 原始太阳星云条件下Fischer-Tropsch反应中的碳同位素分馏 [J]. 中国科学:D辑, 1997, 27（5）: 395-400.]
[47]McCollom T M, Seewald J S. Carbon isotope composition of organic compounds produced by abiotic synthesis under hydrothermal conditions [J]. Earth and Planetary Science Letters,2006, 243: 74-84.
[48]Xue Chunji, Ji Jinsheng, Yang Qianjin. Subvolcanic hydrothermal metallogeny of the Cihai iron (cobalt) deposit, Xinjiang[J]. Mineral Deposits,2000, 19（2）：156-164. [薛春纪, 姬金生, 杨前进. 新疆磁海铁（钴）矿床次火山热液成矿学[J]. 矿床地质, 2000, 19（2）：156-164.]